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Formación del relieve

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Formación del relieve

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Formación del relieve. Factores endógenos

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About Fill in the Blanks
historia
1º e.s.o.
orogenia
 Recommended age: 12 years old
4 times made

Created by

Isabel Torres Fabero
Isabel Torres Fabero
Spain

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Formación del relieveOnline version

Formación del relieve. Factores endógenos

by Isabel Torres Fabero
1


Orogenia por plegamiento . Se produce al dos placas tectónicas constituidas por materiales , y puede ser de dos tipos :

Si las placas tectónicas están formadas por materiales , se pliegan . De este modo , dan lugar a grandes .

En algunos casos , una placa puede introducirse debajo de la otra , lo que genera un proceso denominado plegamiento y .

Orogenia por falla . Al dos placas formadas por materiales , estos no pueden plegarse , por lo que se y producen terremotos . Este proceso da lugar a un relieve con unos bloques y otros .

Orogenia volcánica . Se genera cuando dos placas tectónicas se y dan origen a una zona de volcanes . A través de ellos , los materiales fundidos del manto , que , al , forman y conos .

 
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